吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (6): 1714-1722.doi: 10.13278/j.cnki.jjuese.20180220
林颖典, 刘雅钰, 袁野平
Lin Yingtien, Liu Yayu, Yuan Yeping
摘要: 异重流在自然环境界及工程应用中广泛存在。本文于线性层结及非层结盐水中开展了一系列实验,对开闸式异重流通过植被群的发展和演变特性进行了研究。采用高速相机对异重流头部位置、头部速度和掺混系数等进行了分析,结果表明:异重流在层结水体中头部速度明显减小;层结水体和植被对异重流掺混均有抑制作用;当层结水体和植被同时存在时,异重流的掺混程度与植被高度和水深之比α相关,当α=0.43时,异重流的掺混最为剧烈。本研究也利用粒子图像测速仪(particle image velocimetry,PIV)对异重流局部区域的速度场和涡度场进行研究,结果显示,层结环境抑制异重流正负涡度场发展,但当α=0.20时,即一部分异重流爬上植被顶部时,层结水体与植被的协同效应对跃上植被顶端的异重流下界面涡度有强化作用。
中图分类号:
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[1] | 夏景生, 王志坤, 王海荣, 薛林, 王恺, 刘成权. 渤海湾盆地南堡凹陷西斜坡中深层“混合型河口坝”成因及沉积学意义[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1642-1653. |
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